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Chemical Oceanography
The study of the distribution of elements, isotopes, + compounds in the oceans + the changes that occur.
Marine Chemistry
Focused more on chemical reactions than on the processes determining the distribution of substance in the ocean.
CO2 Gas
The only carbon that has a direct influence on the atmosphere/climate.
Marine Biogeochemistry
Focused on the partitioning + cycling of elements/compounds between living/nonliving parts of an ecosystem (+ connection).
4 CO2 Reservoires
1) Oceans - 38 000 Gt
2) Land - 6 000 Gt
3) Atmosphere - 800 Gt
4) Sediments
Carbon Reservoirs
A series of carbon storage areas that exhibit the continuous transfer of material in different magnitudes + sizes.
Challenger
The first oceanographic expedition over 68 890 miles and 362 days.
Water Samplers
Tubes used for chemical analyses at various depths - can be deployed in groups/sets at various depths for various scientists.
Components of Modern Oceanography
1) International marine research
2) International multi-year programs
3) Submarine technology
4) Satellites (GPS + platforms)
5) Computational modelling
6) Deep ocean drilling
Submersibles
The most used submarine technology but is expensive.
AUVs
Limited by control and are dependent on planning/programming.
ROVs
The most abandoned submersible technology that is limited by a tether (decreasing depths reached and adding drag).
Satellites
Dedicated sensors for physical, biological, geological, and chemical oceanography implications (geolocation/GPS + data collection - buoys/AUVs).
ARGO Floats
Move up and down in the water column at various depths + relays data to satellites repeatedly.
Sediment Traps
Concentrate + collect material from the water column in a filter.
Underwater Observatories
Create ocean networks for data collection (ex. BC, CBS/Holy Rood).
Geospatial Observing Systems
Combines many technologies to provide a clear picture of the processes occurring in the ocean (ex. VENUS).
Stable Isotopes
A newer technique used to track different biogeochemical processes today + in the past.
Stable Isotopes Today
Provide information about the origin of water/organic matter + the biological flow (cycles) of carbon and other elements.
Past Stable Isotopes
Acquired via sediment sampling (piston corers) + deep ocean drilling providing insight into paleoceanography and the chemistry of past oceans/climate